Towler, John. The Silver Sunbeam. Joseph H. Ladd, New York: 1864. Electronic edition prepared from facsimile edition of Morgan and Morgan, Inc., Hastings-on-Hudson, New York. Second printing, Feb. 1974. ISBN 871000-005-9
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THE specific gravity of a body is the comparison of the weight of a given balk of the said substance with that of an equal bulk of distilled water at 62° Fahrenheit. Gases are compared either with air as the standard or with distilled water.
The specific gravity of a body is taken by special instruments for this purpose; some of these instruments are denominated Hydrometers, and give arbitrary indications, which have to be reduced afterward in terms of specific gravity.
Baumé's Hydrometers axe in extensive use in France, and Twaddell's Hydrometer in England. Baumé has two Hydrometers: one for liquids heavier than water, and one for liquids lighter than water.
Deg | Sp. Grav. | Deg | Sp. Grav. | Deg | Sp. Grav. | Deg. | Sp. Grav. |
0 | 1.000 | 20 | 1.152 | 40 | 1.357 | 60 | 1.652 |
1 | 1.007 | 21 | 1.160 | 41 | 1.369 | 61 | 1.670 |
2 | 1.013 | 22 | 1.169 | 42 | 1.381 | 62 | 1.689 |
3 | 1.020 | 23 | 1.178 | 43 | 1.395 | 63 | 1.708 |
4 | 1.027 | 24 | 1.188 | 44 | 1.407 | 64 | 1.727 |
5 | 1.034 | 25 | 1.197 | 45 | 1.420 | 65 | 1.747 |
6 | 1.041 | 26 | 1.206 | 46 | 1.434 | 66 | 1.767 |
7 | 1.048 | 27 | 1.216 | 47 | 1.448 | 67 | 1.788 |
8 | 1.056 | 28 | 1.225 | 48 | 1.462 | 68 | 1.809 |
9 | 1.063 | 29 | 1.235 | 49 | 1.476 | 69 | 1.831 |
10 | 1.070 | 30 | 1.245 | 50 | 1.490 | 70 | 1.854 |
11 | 1.078 | 31 | 1.256 | 51 | 1.505 | 71 | 1.877 |
12 | 1.085 | 32 | 1.267 | 52 | 1.520 | 72 | 1.900 |
13 | 1.094 | 33 | 1.277 | 53 | 1.535 | 73 | 1.924 |
14 | 1.101 | 34 | 1.288 | 54 | 1.551 | 74 | 1.949 |
15 | 1.109 | 35 | 1.299 | 55 | 1.567 | 75 | 1.974 |
16 | 1.118 | 36 | 1.310 | 56 | 1.583 | 76 | 2.000 |
17 | 1.126 | 37 | 1.321 | 57 | 1.600 | ||
18 | 1.134 | 38 | 1.333 | 58 | 1.617 | ||
19 | 1.143 | 39 | 1.345 | 59 | 1.634 |
Deg | Sp. Grav. | Deg | Sp. Grav. | Deg. | Sp. Grav. | Deg | Sp. Grav. |
10 | 1.000 | 23 | 0.918 | 36 | 0.849 | 49 | 0.789 |
11 | .993 | 24 | 0.913 | 37 | 0.844 | 50 | 0.785 |
12 | 0.987 | 25 | 0.907 | 38 | 0.839 | 51 | 0.781 |
13 | 0.980 | 26 | 0.901 | 39 | 0.834 | 52 | 0.777 |
14 | 0.973 | 27 | 0.896 | 40 | 0.830 | 53 | 0.773 |
15 | 0.967 | 28 | 0.890 | 41 | 0.825 | 54 | 0.768 |
16 | 0.960 | 29 | 0.885 | 42 | 0.820 | 55 | 0.764 |
17 | 0.954 | 30 | 0.880 | 43 | 0.816 | 56 | 0.760 |
18 | 0.948 | 31 | 0.874 | 44 | 0.811 | 57 | 0.757 |
19 | 0.942 | 32 | 0.869 | 45 | 0.807 | 58 | 0.753 |
20 | D.936 | 33 | 0.864 | 46 | 0.802 | 59 | 0.749 |
21 | 0.930 | 34 | 0.859 | 47 | 0.798 | 60 | 0.745 |
22 | 0.924 | 35 | 0.854 | 48 | 0.794 | 61 | 0.741 |
The degrees on Twaddell are converted into equivalent specific gravities by multiplying them by 5 and adding 1000; then mark off then mark off three figures as decimals.
Deg | Sp. Grav. | Deg | Sp. Grav. | Deg | Sp. Grav. | Deg | Sp. Grav. | |
1 | 1.005 | 8 | 1.040 | 15 | 1.075 | 22 | 1.110 | |
2 | 1.010 | 9 | 1.045 | 16 | 1.080 | 23 | 1.115 | |
3 | 1.015 | 10 | 1.050 | 17 | 1.085 | 24 | 1.120 | |
4 | 1.020 | 11 | 1.055 | 18 | 1.090 | 25 | 1.125 | |
5 | 1.025 | 12 | 1.060 | 19 | 1.095 | 26 | 1.130 | |
6 | 1.030 | 13 | 1.065 | 20 | 1.100 | 27 | 1.135 | |
7 | 1.035 | 14 | 1.070 | 21 | 1.105 | 28 | 1.140 |
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